Number of the records: 1  

Evolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe)

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    SYSNO ASEP0330111
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleEvolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe)
    Author(s) Rajchl, M. (CZ)
    Uličný, David (GFU-E) ORCID, RID
    Grygar, R. (CZ)
    Mach, K. (CZ)
    Source TitleBasin Research - ISSN 0950-091X
    Roč. 21, č. 3 (2009), s. 269-294
    Number of pages26 s.
    Languageeng - English
    CountryGB - United Kingdom
    KeywordsCenozoic Most Basin ; continental rift ; Eger Graben
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsIAA3012705 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    GA205/01/0629 GA ČR - Czech Science Foundation (CSF)
    GA205/06/1823 GA ČR - Czech Science Foundation (CSF)
    CEZAV0Z30120515 - GFU-E (2005-2011)
    UT WOS000266171900001
    DOI10.1111/j.1365-2117.2008.00393.x
    AnnotationThe Oligo-Miocene Most Basin is the largest preserved sedimentary basin within the Eger Graben, the easternmost part of the European Cenozoic Rift System (ECRIS). The basin is interpreted as a part of an incipient rift system that underwent two distinct phases of extension. The first phase, characterised by NNE–SSW- to N–S-oriented horizontal extension between the end of Eocene and early Miocene, was oblique to the rift axis and caused evolution of a fault system characterised by en-échelon-arranged E–W (ENE–WSW) faults. These faults defined a number of small, shallow initial depocentres of very small subsidence rates that gradually merged during the growth and linkage of the normal fault segments.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2010
Number of the records: 1  

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